Hoh Xil lies in the heart of the Qinghai-Tibet Plateau, with an average elevation of over 4,600 meters. Its highest peak is Bukadaban Peak (also known as Xinqing Peak or Monomah Peak) on the northern edge of the Kunlun Mountains, at an altitude of 6,860 meters; its lowest point is Baozi Gorge (where the Hongshui River crosses through a bend at the southern foot of the Kunlun Mountains), at an altitude of 4,200 meters. The terrain within the area is higher in the north and south, lower in the middle, higher in the west, and lower in the east. The Hoh Xil Mountain Range and the Dongbule Mountain Range traverse the central part of the area, with two broad valley-lake basin belts between the mountains, where the terrain is relatively flat. Mountainous areas above 5,500 to 6,000 meters have developed modern glaciers. Examples include Bukadaban Peak (6,860 meters) and Malan Mountain (6,813 meters). A few peaks exceeding 5,600 meters also have small-scale glaciers, such as Donggangzhari (5,882 meters), with a total glacier area of more than 1,700 square kilometers.
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